The response of North American precipitation during the Last Glacial Maximum due to stationary waves in PMIP3 simulations

• Main Author: Lee, Hung-I
• Format: Text
• Language: unknown
• Published: Zenodo 2020
• Subjects: Ice Sheet
• Online Access: https://dx.doi.org/10.5281/zenodo.3674223; https://zenodo.org/record/3674223

The dataset includes PMIP3 (with the Last Glacial Maximum and Pre-Industrial Control), LMDZ simulations, and the pollen reconstructed proxies. : {"references": ["Bartlein, P., Harrison, S., Brewer, S., Connor, S., Davis, B., Gajewski, K., . . . others (2011). Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis. Climate Dynamics, 37 (3-4), 775{802.", "Beghin, P., Charbit, S., Dumas, C., Kageyama, M., and Ritz, C., 2015. How might the North American ice sheet influence the northwestern Eurasian climate?, Clim. Past, 11, 1467-1490, doi:10.5194/cp-11-1467-2015.", "Braconnot, P., Harrison, S. P., Otto-Bliesner, B., Abe-Ouchi, A., Jungclaus, J., & Peterschmitt, J.-Y. (2011). The paleoclimate modeling intercomparison project contribution to cmip5. CliVAR Exchanges, 56 (16), 15{19."]}